التعرجات النهرية لنهر دجلة في ناحية العلم

Abstract EN

The river canal, which is a lot of diversions, is a pattern of river canal patterns that characterize the river in the stages of maturity and aging.

It is known that the fusillating channels are composed of rocky materials that are separated by weathering and sculpting operations and may consist of rough, incoherent materials such as sand and gravel.

Excess ratio of clay and clay, while soft formations form the bottoms of river canals.

The nature of rock formations in terms of size and cohesion is of great importance in determining the characteristics of the riverbed.

For example, incoherent coarse formations are subject to collapse by lower water degradation at a much faster rate than soft, cohesive formations that typically resist lateral collapses